Dependence of Ice Crystal Size Distributions in High Ice Water Content Conditions on Environmental Conditions: Results from the HAIC-HIWC Cayenne Campaign
Dependence of Ice Crystal Size Distributions in High Ice Water Content Conditions on Environmental Conditions: Results from the HAIC-HIWC Cayenne Campaign
复制标题
高冰水含量条件下冰晶尺寸分布对环境条件的依赖性:HAIC-HIWC 卡宴活动的结果
DOI:
10.1175/jas-d-22-0008.1
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发表时间:
2022
影响因子:
3.1
通讯作者:
Schwarzenboeck, Alfons
中科院分区:
文献类型:
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作者:
Hu, Yachao;McFarquhar, Greg M.;Brechner, Peter;Wu, Wei;Huang, Yongjie;Korolev, Alexei;Protat, Alain;Nguyen, Cuong;Wolde, Mengistu;Schwarzenboeck, Alfons
A new method that automatically determines the modality of an observed particle size distribution (PSD) and the representation of each mode as a gamma function was used to characterize data obtained during the High Altitude Ice Crystals and High Ice Water Content (HAIC-HIWC) project based out of Cayenne, French Guiana, in 2015. PSDs measured by a 2D stereo probe and a precipitation imaging probe for particles with maximum dimension (Dmax) > 55μm were used to show how the gamma parameters varied with environmental conditions, including temperature (T) and convective properties such as cloud type, mesoscale convective system (MCS) age, distance away from the nearest convective peak, and underlying surface characteristics. Four kinds of modality PSDs were observed: unimodal PSDs and three types of multimodal PSDs (Bimodal1 with breakpoints 100 ± 20μm between modes, Bimodal2 with breakpoints 1000 ± 300μm, and Trimodal PSDs with two breakpoints). TheTand ice water content (IWC) are the most important factors influencing the modality of PSDs, with the frequency of multimodal PSDs increasing with increasingTand IWC. An ellipsoid of equally plausible solutions in (No–λ–μ) phase space is defined for each mode of the observed PSDs for different environmental conditions. The percentage overlap between ellipsoids was used to quantify the differences between overlapping ellipsoids for varying conditions. The volumes of the ellipsoid decrease with increasing IWC for most cases, and (No–λ–μ) vary with environmental conditions related to distribution of IWC. HIWC regions are dominated by small irregular ice crystals and columns. The parameters (No–λ–μ) in each mode exhibit mutual dependence.